Method and apparatus for determining the concentration of moisture in materials



Oct. 3,1944. A. ALLEN ET AL 2,359,278

METHOD AND APPARATUS FOR DETERMINING THE CONCENTRATION OF MOISTURE IN MATERIALS Filed Feb. 12, 1941 4 Sheets-Sheet 1 Thai.

DZQY 50w g M 2 WW):

m I T??? INVE TOR A7156???" LEN 5b amt/$ {/ATTORNE Oct. 3, 1944. A. ALLEN ETYAL CONCENTRATION OF MOISTURE IN MATERIALS Filed Feb. 12, 1941 4 METHOD AND APPARATUS FOR DETERMINING THE Sheets-Sheet 2 INVENTOR 44 552? 7- 144 4; EN

14/ mesa H fi anna Oct; 3, 1944. A; ALLEN ETAL 2,359,278

METHOD AND APPARATUS FOR DETERMINING THE CONCENTRATION OF MOISTURE IN MATERIALS Filed Feb. 12, 1941 4 Sheets-Sheet 3 OPPOSL'D INVENTOR 7 141.5507- ALLA'M MARKED ll. Home,

Patented Oct. 3, 1944 7 UNITED STATES PATENT OFFICE METHOD AND APPARATUS FOR DETERMIN- ING THE CONCENTRATION OF MOISTURE IN MATERIALS Albert Allen and Wilfred H. Howe, Sharon, Mass, assignors to The Foxboro Company, Foxboro, Mass, a corporation of Massachusetts Application February 12, 1941; Serial No. 378,648

26 Claims.

This invention relates to a method and apparatus for measuring the vapor pressure exerted by a fluid, or the concentration of moisture in a material by utilizing pressure exerted by the vapor of the fluid, and more particularly to novel method and apparatus for measuring and inutilizing such measurements for indicating, or

recording purposes.

The many objects and advantages of the present invention may best be'appreciated by referring to the accompanying drawings which illustrate several specific embodiments oi the invention. In the drawings:

Figure l is a diagrammatic view of one embodiment of the invention in which a responsive element is heated by convection and radiation;

Figure 2 illustrates a second embodiment of the invention in which the responsive element is heated by electricity;

Figure 3 is an enlarged view partly in section of the responsive element of Figure 2;

Figure 4 illustrates the invention as embodied in a controller; v

Figure 5 illustrates the invention as applied to theproblem of measuring the moisture content of a running web:

Figure 6 is a perspective oi the hygrometer shoe of Figure 5 showing the arrangement of the responsive elements; and

Figure 7 is an axial section through one of the elements of Figure 6.

To aid the reader in understanding the method of the invention and the operation of the novel apparatus shown in the drawings, a brief discussion of the theory of operation is included at this point with special reference to Figure 1 which shows a relatively simple embodiment of the present invention as applied to the problem of measuring the moisture content of air under atmospheric conditions. It is a well known fact that under such conditions the air exerts a pressure, commonly called atmospheric pressure, on any object with which it is in, contact and that if water vapor is present in the air a part of the atmospheric pressure is exerted by the water vapor content. This partial pressure of water vapor may be taken as a measure oi the volume of water vapor in the air. For example, if the atmosphere contains 1% by volume of water vapor, the partial pressure exerted by the water vapor will be 1% of the total atmospheric pressure The method here used to measure the moisture content of air consists generally in artificially producing a vapor pressure suflicient to balance the partial pressure of water vapor in the atmosphere and effectively measuring that artificially produced pressure by measuring the value of a condition which varies with changes in the value of the artificially produced pressure.

' It is known that there are substances that have the characteristic of taking on the vapors of liquids and that the vapors have a tendency toescape again to the circumambient surroundings, and that this escaping tendency, which.

may be measured in terms of vapor pressure, increases with other physical conditions of the substance such, for example, as increasing temperature. Examples of such substances are certain salts such as lithium chloride and calcium chloride which are hygroscopic, that is, they have a tendency under certain conditions to take up water from the atmosphere. The water associated with the salt has a tendency to escape to the atmosphere again and this escaping tendency, whichmay be measured in terms of vapor pressure, increases with increasing temperature. when such a salt is heated, a temperature is eventually reached such that the escaping tendency of the water associated with the salt is just equal to the tendency of thesalt'to take on water from the atmosphere. In other words, the vapor pressure exerted by the water associated with the salt is equal to the partial pressure of water vapor in the atmosphere and an equilibrium. condition exists such that the quantity of water taken up by the salt from the atmosphere is just equal to the quantity of water given up by the salt to the atmosphere. At this equilibrium point the temperature of the salt and the water associated therewith is a; measure of the partial pressure of water vapor in the surrounding atmosphere.

Referring now to Figure 1 of the drawings, the

numeral l indicates an open pan containing a quantity or lithium chloride 2. The pan l is supported at one endoi a lever 3 which .itself is freely pivoted about a fulcrum 4. At its other end lever 3 is provided with an indicating pointer 5 which cooperates with an index or scale 8. The pointer indicates on the scale the distance between the pan and a suitable source of constant temperature heat such asthe stove I, and consequently the pointer effectively indicates the temperature of the salt. Lever 3 is provided-as shown with a counterweight to balance the weight of the pad I and salt thereon.

With the apparatus disclosed. the temperature of the salt; 2 is automatically maintained at an equilibrium value such that the amount of water which the salt'absorbs from the circumambient atmosphere is equal to the amount-oi water given up by the salt to theatmosphere. This automatic adjustment is accomplished in the following manner. 1

If the pan i is so located with respect to the heater 1 that the salt 2 is at its equilibrium temperature and an increase in the moisture content of the circumambient' atmosphere occurs, the salt 2 will begin to take on water from theatmosphere. The resulting increase in the weight of the salt will cause the pan tomove downwardly toward the heater thus increasing the temperature, of the salt. The'increase in temperature of the salt becomes sufllcient to cause.

the salt to stop taking-moisture from the atmosphere and to lose such moisture as is neces sary to return the salt to its original weight (the weight at which it balances counterweight to) so that the pan may reach a position of balance with respect to the heater at such a point that "a new equilibrium temperature is established corresponding to the new moisture condition of the atmosphere. With a decrease in atmospheric moisture content, the operations described above a. measuring instrument 20, such as a wattmeter,

be advantageously heated by passing an electric current therethrough. A length of wire or nar-- row metallic strip i6 -is helicaily wound around the exterior of the saline wick and is connected by the conductor H to one terminal of the secondary of a suitable transformer IS. The other terminal of the secondary of the transformer I! is connected by conductor ll to the flexible cable I! near the temperature sensitive bulb I 4, thus completing a circuit through bulb i4, saline wick Ii, and wire helix I. If desired, an electrical may be connected in the circuit as shown.

. The transformer II is connected to a suitable source of ll0-volt BO-cycle power. It is usually desirablev to use alternating current to reduce the tendency oi the salt solution on the-saline wick to electrolyze and decompose; The wire it and bulb I4 may. advantageously be constructed of silver which combines the properties or high electrical conductivity and eilective re- It may be observed that the weight of the salt does not of itself .bear any necessary relationto the" moisture content of the circumambient atmosphere. Weight merely exemplifies a condition or characteristic'of the salt which be conveniently used to control the heat supply to ing is accomplished by supplying electrical en's may directly to the sensitive element and wherein variations in resistance rather-than variations in weight mines to control the heat supply tomaintain a salt at equilibrium tem} perature. Referring tmrigurz. a conventional recording thermometer. H is by-a deslution with which thesaline wick is impregnated sistance to th corrosive tendencies of the saline solution. The wick proper may be made 01 any suitable fibrous material such as cotton, asbestor,

The potential of the electrical energy supplied tothe wick may be varie'd considerably but it is necessarytosupply a'certain minimum potential. This minimum potential will vary, with the character of the saline wick used, but should be sufiicient to raise the .temperature of the saline. wick to itsoperative range, that is, at least to the equilibrium temperaturereferred to. above. With the apparatus above described good results have been obtained with a potential of 10 volts using .025" diameter wire for wrapping the wick II and spacingthe'turns to give ten turns in the inch.

The operationof the device is as follows: As

pointed out above, the electrical conductivity oif the saline wick II is a function'of the quantity oi'water associated with the lithium chloride on wick. 'Asthe wetn'u s ot thesaline wick in-v creases, its conductivity increases also, and vice v'ersa. As'elec cal energy (PR) is supplied to thoclement II, and hence the-vapor pressure exerted by the sowill when the temperature has risen ible cable .12 to a sensitive element generally intive bulb ll wrapped in a wick-ll. This wick is treated with a saturated solution-of lithium chloride til-disperse the lithium chloride thro lih out the fibers of the wick, preferably in such a manner thatin subsequent usecsome' undissolved'salt is always present on. the wick; The

. wick-thustreated'will be referred to asa salino wick and as suchwhencontaining moisture has dicated at n. ("rue element is may serum to to as a "hot bulb.") As best-shown" in Iflgure 3-.-

' the element It comprises atemperature sensir 7 tothepointwherethovaporpressureexertedby the' water of the lithium chloride solution equals the partial pressure of water vapor in the circumambientatmosphere, the equilibrium condition' referred to above is reached and thereafter -'tbe,temperature will be automatically maintained at that point.- If the-temperature of the sensitive element II and lithium chloride solution is above the equilibrium tem ture. the saline yick will give up water to the atmosphere and "continue to dry out until its conductivity dc current tothe saline wick decreases to lower the the property of conducting electricity.

creases in the pointv where the flow or heating temperature of the element to the equilibrium value. If,-"o n the other hand, the temperature of the saline wick and solutiondmps below'this equilibrium point, the lithiumchloride will take upiwater from the atmosphere. the conductivity of the saline wick will increase, and hence the flow of heating current through the saline will increase to increase theteniperaturoof sensitive element. Thus the equilibrium telns temperature will tend torise perature of the element It is automatically maintained at the desired value and may be used to measure the moisture content of the circumambient atmosphere.

The recording thermometer ll may be calibrated to read directly in terms of moisture content, that is, to indicate the percent by volume of water vapor in the atmosphere. Under certain circumstances an indication of moisture content maybe obtained by measuring the heat supplied to the responsive element It by measuring by means of the instrument II the quantity of electrical energy supplied to the saline wick ii to heat it.- However, in most cases it is desirable to measure the temperature of the saline wick directly by a recording thermometer as shown, or by a thermocouple or other temperature measur- 7 ing device.

Under certain circumstances it may be desirable to know the moisture contentoi an atmosphere in terms of percent relative humidity rather than in terms of absolute humidity. By percent relative humidity is meant the ratio .01

the quantity oi water actually present in the atmosphere to the quantity of water that would be present in the atmosphere ii it were saturated at the ambient temperature, multiplied by one hundred. It can be mathematically shown that such suitably located in the room or other space wherein the relative humidity is to be controlled. Element 22:: like the element I3 is supplied with electrical energy from a suitable source such as a transformer 24 and is connected by a flexible cable 23a with a pressure responsive helix 2 which tends to unwind and wind up as the temperature of element 22a rises and falls. Element 22b, which measures ambient atmospheric temperature, receives no supply of electrical energy and is connected by flexible cable 23b with a pressure responsive helix 25 similar to the helix 28. (For convenience in distinguishing elements 22a and 22b, they may be referred to, respective- 1!], as the "hot bulb" and "dry bulb.) Helix 25 through lever 21 and link 28 actuates a' bell crank a value for percent relative humidity can be obtained by suitably correlating the value oi. absolute humidity as represented by the temperature of the sensitive element ll (Figure 2) and the value of the ambient temperature as measured by any suitable means. Whereas there are 'several such relationships that may be used, one that lends itself to commercial practice is that in which the diilerence between the temperature of the sensitive element It and the temperature oi the circumambient atmosphere is utilized to indicate relative humidity. Such a temperature diiierence may be obtained with a relatively simple mechanical linkage system. Although the accuracy of the indication of relative humidity obtained in this way varies slightly with changes in ambient temperature, commercially satisfac-' tory results may beobtained in many cases without compensation for changes in ambient temperature, especially where the variations in ambient temperature are relatively small. The indicating element oi the recording thermometer may be made responsive to the diil'erence between the temperature of the saline wick l5 and the temperature of the ambient atmosphere and the instrument may be calibrated to read directly in terms of relative humidity. Furthermore, either the temperature of the, wick ill or the temperature difference between the saline wick i5 and the atmosphere may be used as a control variable to control either the absolute humidity or the relative humidity oi an atmosphere as will now be described.

Referring now to Figure 4 of the drawings and particularly the lower right-hand portion 01' Figure 4, there is shown a water supplypipe H which supplies water for humidiiying a room or other space to be humidified in' known manner. The pipe 11 is provided with apneum'atically operated control valve [5 and the rate of flow of water in pipe 11 is controlled by varying the air pressure supplied to the valve I5 in a manner now to be described.

Referring to the upper right portionoi Figure 4, there are shown two temperature-sensitive elements 22a and 2% which may be constructed like the element l3 oi Figure 2 and which may be lever pivoted at 30 and comprisingthe arms 29a and 29!). Connected to, moving with, and supporting the bell crank 29a, 29b is an arbor 3| carrying a pen arm 32 which records the temperature measured by ambient. temperature element 22b. The element 26 through lever 33 and link 34 moves a bell crank lever pivoted at 8! and comprising the arms 35a and up. Connected to, moving with, and supporting bell crank 35a, 35b is an arbor 31 carrying the pen arm 38 which records the temperature measured by the element 22a. The arm 29b of bell crank 29 is provided with a yoke 39 which holds a spindle 39a plvotally supporting a differential lever ll, one end of which is positioned by a tongue ll extending from the arm 35b of bell crank lever 35a, 35b.

The other end of lever 40 may be used to operate control mechanism of any desired type and such operation would make the control mechanism responsive to the difierential action of the two bulbs 22a and 22b. For purposes of illustration a controller such as disclosed in the Masonreissue Patent No. 20,092 may be used, in which event the differential lever would be connected to operate a baille of the control couple disclosed in the Mason patent. Such control mechanism is diagrammatically shown in Figure 4 and comprises a pair of opposing bellows i9 .ior operating a nozzle 49 in conjunction with a baiile 4'' cperated by the lever 40. It also includes a relay valve 62 pneumatically operated by the output pressure of the nozzle and baille to control the supply of air pressure to and from the opposing bellows 59. As disclosed in the Mason patent the opposing bellows are connected through a restriction 65. The operation 01 this control structure will not be described here since it forms no part of the present invention and is fully disclosed in the Mason patent. It is deemed sufllcient'to point out that through the operationoi' the control mechanism the pneumatically operated valve II controls the water supply to the humidiiying apparatus so as to maintain substantially constant the temperature difference between the two bulbs 22a and 22b.

The desiredvalue of relative humidity (the control point) may be varied by adjusting the neutral position of nozzle 49. This adjustment perature measurement.

a steam line I03 and branch lines I04 and llll. Near the point where the cotton w'arp I leaves the roll III and between the warp and roll I02,

flexible cable I01 to a recording instrument I08. The shoe M8 is shown more in detail in Figure 6 and comprises a rectangular metal shell Ill forming a compartment 2 which is enclosed on all sides except the side which is exposed to the warp I00. Compartment! contains the responsive elements I09 (hot bulb) and 0 (dry bulb) which. in this embodiment, are shown as using electrical resistance thermometers for tem- The elements i0! and llllmay be similarly constructed and may be made as shown in Figure 7.

Referring to Figure '7 which shows a section through one of the elements. a double layer I28 of insulated nickel resistance wire is wound on a hollow wooden core ill, the resistance wire leads being designated as I22 and I23. A silver conductors .IN and I28 with electrical heating energy whereas the element Ill, although similarly constructed, receives no supply or heating energy.

Referring again to Figure 5, the flexible cable "I carries six conductors connecting the shoe ill with the instrument I. One pair of conductors supplies heating energy to the leads I24 and' Ill, and one pair 01' conductors is connected to the resistance elements of each or elements II! and Ill. The instrument I0! is supplied with electric power i'rom a'suitable source (not shown) and i of a type suitable for recording thediirerence in. temperature between the electrical resistances of elements I" and HI. Such apparatus is well known in the art and will not be described in detail here. The resistances may. for example, be connecteddn'two arms. of an electrical bridge circuitins'uch a manner that a galvan'ometer connected across the bridge circuit indicates the temperature diflerence beopen helix. The element I" is supplied through 40' tion.

tweeh the elements. The apparatus may be oi I The operation or the sm lls audits associated elements is as follows: In drying iibrous materials or a given type, the moisture contained In such a case a lmeumati 9,359,278 m which are heated by steam passing through solution with which the paper In is impregnated just equals. the pressure 01' water vapor in the surrounding atmosphere, and hence the 'vapor pressure of the water contained in the warp passing the shoe I08. The element H0, since it has no electrical heating connection, will assume the temperature or its surrounding and hence have v the same temperature-as the warp.

As pointed out above, there is a definite relationship between the moisture content of a warp of given materiaL'its temperature, and the water vapor pressure which it exerts. This relationship can be determined and the actual moisture content 01' the material may be determined by properly correlating measured values of its temperature and water vapor pressure. In the present embodiment, the diiierence between a tempef ature corresponding to the water vapor pressu e of the warp (temperature'ot the element I08) and the temperature oithe warp (temperature of the element H0) is used as a measure of the moisture content oi the warp. We have found that the temperature diirerence between the elements I09 and llll is a reasonably accurate measure of moisture content c! warp material within the usual working range with limited temperature variations. For wider temperature variations the general relationship holds, but cor rection must be applied both for the amount of temperature variation and the rate of change of temperature for given moisture changes, the amount of the correction depending upon the deviation of the temperature. Furthermore, the temperature in the compartment H2 is slightly lower than that of the warp although, as stated above, the shoe I" is so constructed as to'minimize this difl'erence. However, this latter temperature diilerence is roughly constant and hence enters as a'constant correction in the calibra- The instrument It! may. if desired,-'be calibrated to read directly in terms of warp moisture content.

It will be understood that the instrument Ill tent of the warp may be controlled by controlling the flow of steam to heat the rolls llll and I". 11y operated control valve ll may be inserted in the pipe I" and the valve Ill may be connected by a pipe ill withthe instrument I" in known manner.

7 As pointed out above, the foregoing description is of specific embodiments of the present invention. The scope or possible application or the present invention is so wide and the number that might be,

of possible equivalent elements substituted for the elements described above so in the fibers at their existing temperature develops a definite water vapor pressure characteristic of that temperature and moisturecontcnt.

Since the .warp ill continuously moves past the open faceof compartment III, the space within the compartment will quickly reach a condition of temperature and water vapor pressure the same as that of the warp. The shoe ill is preterably constructed so that by contacting the warp the temperature of the shoe as a whole will be great that it would clearly be impracticable to include an exhaustive list in this specification. However, it seems desirable at this point .to'indicate a few of the other fields of application of the present invention and some of the elements which mizht be substituted for those illustratively shown inthe drawings Itis first or all apparent that the present invention may be used not only as illustratively shown and described herein to measure the water vapor content or relative humidity or an air atmosphere, but also to mess,-

nearly that r the warp. and the temperature difj "teren'ce between the warp, and compartment .l I!

' wiil'b'e a minimum.

' The element I", like the element It of 2," is supplied with electrical heating energy and hence its temperature rise to apol'nt Wh re the vaporpressureoithe; water in the saline are the moisture content of other mixed vaporatmospheres or to measure the proportion of constituents other than water vapor present in a vapor atmosphere, or to measure the pressure or a vapor or gas which is'the sole component of an atmosphere. It may also be used tomeasure the fiuid concentration in a solid material as disasoaavs stituent for the mediumis essentially a function a I 01' temperature and a characteristic of the medium capableof influencing flow or heat energy thereto is a function of the quantity oi the measured constituent associated with the medium.

Furthermore, the method of the present inventlon presents numerous advantages over preexisting methods of measuring one constituent of a mixed atmosphere. For example, one method oi measuring thehumidity of an atmosphere is by the use of a so-called wet and dry bulb thermometer. The accuracy of such a device depends in large measure upon -adequate circulation of air or other atmosphere past a moisture responsive element. With a device such as that of Figure 4, accuracy of measurement is substantially independent of the rate of circulation past the responsive element, and accurate measurements may be obtained with only enough circulation past the responsive element to insure that the atmosphere in contact with the element is a representative sample of the whole. With a wet and dry bulb thermometer, a continuous supply of water of high purity is required, whereas the apparatus of the present invention operates without any addition 01' water. It requires only a convenient source of heating energy, and the power requirements are small. Moreover as a humidity measuring device, the device of the present invention may be operated at relatively low ambient temperatures because the ireezin'g point of a saturated lithium chloride solution is substantially below that of water.

The heating of the responsive element may be done by electricity or by a stove as disclosed, or steam orother suitable heating media may be used. The heating may be direct or indirect, that is, the heating may be accomplished as in Figure 2 by passing an electric current directly through the element, or the heating may be indirect as in Figure 1.

We claim:

1. The method of measuring the partial pressure or quantity of moisture present in an atmosphere, comprising the steps of supplying electrical energy to a. medium having a preferential aillnity for said moisture which is a discontinuous Junction of temperature and having anel'ectrieal characteristic capable of influencing flow oi electrical energy in said medium which is a function of the quantity of said moisture associated with said medium to cause a currentto flow in said medium'to heatsaid medium to a critical 'eduilibrium temperature corresponding with the quantity of said moisture in said atmosphere and measuring the temperature or said medium as an'indication of thepartial pressure or quantity of said moisture present in said atmosphere.

2. The method of measuring the humidity of an atmosphere which comprises the steps .01 supplying electrical energy to a wick impregnated with a saturated saline solution to heat the same to an equilibrium temperature corresponding with wick to said atmosphere, and measuring the temperature of said wick as an indication of the humidity of said atmosphere.

, 3. The method of measuring the relative humidity of an atmosphere which comprises supplying electrical energy to a wick impregnated with a saturated saline solution to -ieatthe same to its equilibrium temperature, measuring said equilibrium temperature of said wi.k, measuring the temperature 6f the atmosphere, and subtracting said-atmospheric temperature irom said wick temperature to obtain a value indicative of the relative humidity of said atmosphere.

4. In apparatus for measuring the quantity'oi moisture present in an atmosphere, the combination of a medium having a preferential afllnity for said moisture which is a discontinuous function of temperature and having an electrical characteristic capable ofinfluencing flow of electrical energy in said medium which is a function of the quantity of said moisture'associated with said medium, means for supplying electrical energy to said medium to cause a current to flow therein to heat said medium to a critical equilibrium temperature corresponding with the quantity of said moisture present in said atmosphere, and means responsive to the temperature of said medium to indicate the quantity of said moisture present in said atmosphere.

5. Apparatus for measuring the proportion oi condensible vapor present in an atmosphere, comprising, in combination, a porous medium exposed to said atmosphere and wetted with a saturated saline solution of the condensate of sa.d condensible vapor, means for supplying electrical energy to said medium to cause a current to flow therein to heatsaid medium to an equilibrium temperature corresponding with the proportion of said condensible vapor in said atmosphere, and means for indicating the condensible vapor con-- tent of said atmosphere including an element responsive to the temperature of said medium.

6. Apparatus for measuring the humidity of an atmosphere, comprising, in combination, a wick wetted with a saturated solution of lithium chloride and exposed to said atmosphere, means for supplying electrical energy to said wick to heat the same to an equilibrium temperature corresponding with thehumidity of said atmosphere. and means responsive to the temperature of said wick for indicating the humidity of said atmosphere.

said wick is heated to and maintained at a critical equilibrium temperature corresponding with 'the humidity of said atmosphere, and means responsive to the temperature of said wick for indicating the humidity of said atmosphere.

8. In apparatus responsive to the humidity of an atmosphere, in combination, a humidity responsive element comprising a thermometer bulb, a saline wick substantially surrounding said bulb, and a conductor in contact with the exterior tric current to flow from said conductor through the humidity of said atmospl'iere, exposing said 1 surface of said wick, means for causing an elecsaid wick to said bulb to heat said wick. and means connected to said bulb .ior actuation in accordance with the humidity of said atmosphere.

9. The method of measuring the partial pressure or quantity of water vapor present in anatmosphere comprising the steps of supplying heating energy to a medium having a preferential afilnity for said water vapor up to but not above a critical equilibrium temperature corresponding with the quantity of water vapor present in said atmosphere and having a characteristic capable of influencing flow of heating energy to said medium which is a function of the quantity of water associated with .said medium, the quantity of heating energy supplied to said medium being suihcient to heat it to said equilibrium temperature, and effectively measuring .the temperature of said medium as an indication of the partial pressure or quantity of said water vapor present in said atmosphere.

10. The method or measuring the amount of moisture in a inoist material which comprises exposing to said moist material a medium capable of continuously taking up or giving oi! said moisture-depending, respectively, upon whether the temperature of said medium is below or abovean equilibrium temperature corresponding to the amount of moisture in said material, said medium having .a characteristic which is'a continuous function of the amount of. said moisture held by said medium, supplying heating energy to said medium in accordance with the value of said characteristic to maintain said I medium of said equilibrium temperature, and et- Iectively determining the value of said equilibrium temperature as a measure of the amoun of said moisture in said material.

11. In apparatus for measuring the amount of moisture in a moist material, the combination of a medium capable of taking on and givingoi! said moisture depending on whether the temperature of the medium is, respectively, below vor above an equilibrium value corresponding with the concentration of said moisture in said mateterial, said medium having a characteristic which is a continuous function of the amount of said moisture held by said'm'edium, means for, supplying heating energy to said medium in accordancewith the value of said-characteristic to maintain said medium'at said equilibrium temperature, means for measuring the equilibrium temperature of said medium, and means responsive to the value of said equilibrium temperature for indicating the amount of said moisture in said. material. a

.12..Ihe method oi measuring the concentration 01? water vapor-Vin an atmosphere which comprises exposing to said atmosphere a saline medium comprising a wick impregnated with a saturated salt solution capable of taking up water from said atmosphere or giving up water to said atmosphere according towhether the tenipera-. ture of said wick is, respectively. below orabove content of a solid material which comprises the steps of establishing a moisture exchanging relationship between said solid and a medium capending respectively upon whether the temper ature of said medium is below or above an equilibrium temperature corresponding to the concentration of said moisture in said material, said medium having a characteristic which is a iunction of the amount 0! said moisture held by said medium, supplying heating energy to said medium in response to the value of said characteristic to maintain said medium at said equilibrium temperature, and eflectively determining the value of said equilibrium temperature as a measure of the moisture 'content oi said material.

14. The method or measuring the in a confined space adiacent said web a saline medium capable of taking'up water from said web or giving up water to said web according to-whether the temperature of said medium is respectively below or above an equilibrium temperature corresponding to the concentration of water in said web, supplying electrical energy to said saline medium to heat it to said equilibrium temperature, eflectively measuring said equilibrium temperature, measuring the ambient temperature in said confined space, and determining the diii'erence between said equilibrium temperature and said ambient temperature as a measure of'the moisture content of said web.

15. The method oi measuring the concentratlon oi moisture in a moist material which comprises enposing to said moist material a quantity of a medium capable of taking on or giving oi! said moisture depending respectively upon whether the temperature of said mediumis below or above an equilibrium temperature cdrresponding'to the concentration of said moisture in said material, supplying heat energy to said medium to heat it to said equilibrium temperasaid quantity of medium and the moisture associated therewith, and eflectively determining the value of said equilibrium temperature as a measure of the concentration of said moisture in said material.

16. The method of measuring the concentration of water in a material which comprises exposing to said material a medium. capable of continuously taking up or giving oil water depending respectively upon whether the temperatuie of said. medium is below or above an equilibrium temperature corresponding to the concentration oi water'in said material, said medium having an electrical characteristic which is a function of they amount of water held by said medium, supplying heating energy to said medium in accordance with the value of said electrical characteristic to heat said medium to and maintain said medium at said equilibrium temperature and efiectively determining the value of said equilibrium temperature as a mess- :gliagf the concentration of water in said ma- .17. The method of measuring the concentra-' tion 01' water in a material which comprises ex-' posing to said material a medium capable oi taking up or giving of! water depending respectively upon whether the temperature 01' said medium is below or above sin-equilibrium tmnperature corresponding to the concentration of water in said material, said medium having an pable oi taking up or giving ofl said moisture de- 7 electrical resistance which varies with the moisture content of a running fibrous web-which icomprises continuously exposing to. said web withamount of water held by said medium, supplying electrical energy directly to said medium to maintain said medium at said equilibrium temperature, and effectively determining the value of said equilibrium temperature as a measure of the concentration of. water in said material.

18. The method of measuring the concentration of water in a material which comprises exposing to said material a ,medium capable of taking up or'giving ofi water depending respectively upon whether the temperature of said medium is below or above an equilibrium temperature corresponding to the concentration of water in said material, said medium having a characteristic which is a function of the amount of water held by said medium, supplying heating energy indirectly to said medium under the control of the value of said characteristic to maintain said medium at said equilibrium temperature, and effectively determining the value of said equilibrium temperature as a measure of the concentration of water in said material.

19. The method of measuring the moisture content of a material which comprises exposing to said material a quantity of a medium capable of taking up or giving off moisture depending respectively upon whether the temperature of said medium is below or above an equilibrium temperature corresponding to the concentration of moisture in said material, the weight of said quantity of medium being a function of the amount of moisture held by said medium, supplying heat energy to said medium in response to variations .in the weight of said quantity of medium and the moisture associated therewith to maintain said medium at said equilibrium temperature, and effectively] determining the value of said equilibrium temperature as a measure of the moisture content of said material.

20. In apparatus for measuring the water content of a material by measuring the concentration of water vapor in a. confined space in moisture equilibrium with said material, com prising, in combination, a medium capable of taking up or giving off said fluid depending respertively upon whether the temperature of said 'medium is below or above an equilibrium temperature corresponding to the water content of said material, said medium having an electrical characteristic which is a function of the amount of water held by said medium, means for supplying electrical energy directly to said medium to heat said medium to and maintain it at said equilibrium temperature, and means responsive to the equilibrium temperature of said medium for indicating the concentration of water in said material.

21. The method of measuring the moisture content of a solid material by measuring the concentration of moisture in a confined atmosphere in equilibrium with said moisture-containing solid material which comprises the steps of exposing to said atmosphere a medium capable of taking up or giving of! moisture depending respectively upon whether the temperature-of said medium is below or above an equilibrium. temperature corresponding to the concentration of moisture in said material, said medium having a. characteristic which is a continuous function of the amount of moisture held by said medium, supplying heat energy to said uring said equilibrium temperature and eilectively determining the diflerence between the value of said equilibrium temperature and the value of said ambient temperature as a measure of the concentration of moisture in said solid material. 22. The method or measuring the water content of a material by measuring the concentration of water vapor in a confined atmosphere in vapor equilibrium with said material which comprises exposing to said atmosphere a medium capable of taking up or giving ofi water depending respectively upon whether the temperature of said medium is below or above an equilibrium temperature corresponding to the concentration of water in said atmosphere, said medium having a characteristic which is a continuous function of the amount of water held by said medium, supplying heat energy to said medium in response to the value of said characteristic to maintain said medium at said equilibrium temperature, effectively determining the value of said equilibrium temperature, measuring the ambient temperature of said confined atmosphere, and determining the difierence between said equilibrium temperature and said ambient temperature as a measure of the concentration of water,

in said material.

23. The method of measuring the relative humidity of an atmosphere which comprises exposing to said atmosphere a medium capable 01 taking up or giving ofi water continuously depending respectively upon whether the temperature of said medium is below or above an equilibrium temperature corresponding to the concentrationof water vapor in said atmosphere,

, ature and the value of said ambient temperature to obtain an indication of the relative humidity of said atmosphere.

'24. The method 01' measuring the moisture content'of a running fibrous web which'comprises continuously exposing to said web within a confined space adjacent said web a saline medium capable of continuously taking up water from said web or giving up water to said web according to whether the temperature or said medium is respectively below or above an equilibrium temperature corresponding to the concentration of water in said web, supplying electrical energy to said saline medium to heat it to said equilibrium temperature effectively measuring said equilibrium temperature, measuring the ambient temperature in said confined space, and correlating said equilibrium temperature and said ambient temperature to obtain a value indicative of the moisture content of said web.

25. In apparatus for measuring the moisture content of a running web, in combination, a chamber having an opening, means for continually causing said web to pass said opening, a saline medium in said chamber capable of taking on water from said web or giving up water to said web, depending respectively upon whether the temperature of said medium is below or above an equilibrium temperature corresponding to the moisture concentration of said web, means for supplying heat energy to said saline medium to bient temperature and the value or said equilibrium' temperature .to obtain a value indicative of the moisture content of said web.

26. The method or measuring the amount of moisture present in an atmosphere comprising the steps 0! supplying electrical energy to a medium having an ailinity for said moisture which, at an equilibrium temperature corresponding with the amount of moisture in said atmosphere,

changes a relatively large amount {or a relativelyisiight change in temperature, said me dium also having an electrical characteristic capable of influencing flow of electrical energy in said medium, which is a function of the quantity of said moisture associated with said medium, and the quantity or electrical energy supplied to said medium being suflicient to heat said me-.

dium to said equilibrium temperature, and measuring the temperature 9! said medium as an indication oi the amount of moisture present in said atmosphere. I

' I ALBERT .AILEN.

WILF'RED H. HOWE. 

